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Seismicity before and after the two great Sumatra earthquakes of 2004 and 2005

Wybrane pełne teksty z tego czasopisma
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EN
Abstrakty
EN
The Harvard CMT catalogue contains 481 shallow earthquakes that occurred between 1 January 1977 and 30 November 2005 within a broad region defined by the geographical latitude from 3°S to 14°N and by the longitude from 91°E to 102°E. There are 230 events that occurred before the great earthquake of 26 December 2004. Their surface distribution is not uniform and the source area of the 2004 great event appears as an area of seismic quiescence with a radius of about 100 km. There are 186 events that occurred between the two great earthquakes of 26 December 2004 and 28 March 2005. Practically all of them are located to the northwest from the great earthquake of 2005, that in turn was followed by 63 events, mostly located to the southeast. The cumulative seismic moment from earthquakes before the occurrence of the great event of 2004 increased rather regularly with time, with sudden increase about twenty years and two years before the occurrence of the great event. The seismic moment of earthquakes between the two great events increased rapidly during the first ten-fifteen days, then flattened out and increased slowly with time. After the great event of 2005 the seismic moment shows quiet increase during some 115 days, then sudden jump, followed by very small activity till the end of our observations. From the spatial distribution of seismic moment of earthquakes that occurred before the great event of 2004 it follows that its largest release appeared to the southeast from the great event, around the rupture area of the great earthquake of 2005. The largest release of seismic moment from earthquakes between the two great events is observed in the vicinity of the 2004 event and further up to the north. The seismic moment from earthquakes that occurred after the great event of 2005 was mostly released in its vicinity and further down to the south.
Czasopismo
Rocznik
Strony
343--360
Opis fizyczny
Twórcy
autor
autor
  • Institute of Geophysics, Polish Academy of Sciences ul. Księcia Janusza 64, 01-452 Warszawa, Poland, debski@igf.edu.pl
Bibliografia
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  • Kennett, B.L.N., and P.R. Cummins, 2005, The relationship of the seismic source and subduction zone structure for the 2004 December 26 Sumatra-Andaman earthquake, Earth Planet. Sci. Lett. 239, 1-8.
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  • Lay, T., H. Kanamori, C.J. Ammon, M. Nettles, S.N. Ward, R.C. Aster, S.L. Beck, S.L. Bilek, M.R. Brudzinski, R. Butler, H.R. DeShon, G. Ekström, K. Satake and S. Sipkin, 2005, The great Sumatra-Andaman earthquake of 26 December 2004, Science 308, 1127-1133.
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  • Tsai, V.C., M. Nettles, G. Ekström and A.M. Dziewonski, 2005, Multiple CMT source analysis of the 2004 Sumatra earthquake, Geophys. Res. Lett. 32, 17304,doi: 10.1029/2005GL023813.
  • Vigny, C., W.J.F. Simons, S. Abu, R. Bamphenyu, C. Satirapod, N. Choosakul, C. Subarya, A. Socquet, K. Omar, H.Z. Abidin and B.A.C. Ambrosius, 2005, Insight into the 2004 Sumatra-Andaman earthquake from GPS measurements in southeast Asia, Nature 436, 201-206.
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0014-0070
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